Sensitivity of surface radiation budget to clouds over the Asian monsoon region

Balachandran, S. ; Rajeevan, M. (2007) Sensitivity of surface radiation budget to clouds over the Asian monsoon region Journal of Earth System Science, 116 (2). pp. 159-169. ISSN 0253-4126

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Using the ISCCP-FD surface radiative flux data for the summer season (June to September) of the period 1992 to 1995, an analysis was done to understand the role of clouds on the surface radiation budget over the Asian monsoon region. At the top of atmosphere (TOA) of convective regions of the Asian monsoon region, the short wave radiative forcing (SWCRF) and long wave radiative forcing (LWCRF) do not cancel each other resulting in occurrence of the net cloud radiative forcing values exceeding −30 W/m2. This type of imbalance between SWCRF and LWCRF at TOA is reflected down on the earth surface-atmosphere system also as an imbalance between surface netcloud radiative forcing (NETCRF) and atmospheric NETCRF. Based on the regression analysis of the cloud effects on the surface radiation budget quantities, it has been observed that generally, the variance explained by multiple type cloud data is 50% more than that of total cloud cover alone. In case of SWCRF, the total cloud cover can explain about 3% (7%) of the variance whereas the three cloud type descriptions of clouds can explain about 44% (42%) of the variance over oceanic (land) regions. This highlights the importance of cloud type information in explaining the variations of surface radiation budget. It has been observed that the clouds produce more cooling effect in short-wave band than the warming effect in long-wave band resulting in a net cooling at the surface. Over the oceanic region, variations in high cloud amount contribute more to variations in SWCRF while over land regions both middle and high cloud variations make substantial contributions to the variations in both SWCRF and NETCRF.

Item Type:Article
Source:Copyright of this article belongs to Indian Academy of Sciences.
Keywords:Surface Radiation Budget; Short Wave Radiative Forcing; Long Wave Radiative Forcing; Net Cloud Radiative Forcing
ID Code:94348
Deposited On:05 Sep 2012 11:51
Last Modified:19 May 2016 07:11

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